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Although sharpening was undertaken for spatial resolutions from 990 m to 90 m, root mean square error (RMSE) of <2 K could, on average, be achieved only for 990 270 m in the ASTER data.
Prediction of water levels inside Port Canaveral (Trident Pier) is to within 0.06 m root mean square error and includes the observed forerunner and peak surge of the hurricane.
Simulation results represent the time-series of water surface elevations measured in the open coast off Melbourne Beach (Spessard) within 0.05 m root mean square error and within 12% of observed maximum surge elevation (1.35 m simulated vs. 1.52 m measured) and exhibit details induced by a 'loop' performed by the hurricane before it made landfall.
Largest root spread was in a Year-3 blackwood at 10.3 m with one Year-2 blackwood having 9.0 m root spread.
The moisture holding capacity in the 1 m2 × 1.5 m root zone is assumed 1150 l with a wilting point being 450 l.
Over open areas with relatively flat terrain, it is common to achieve elevation accuracies below 0.15 m root mean square error (RMSE) [22-24].
Similar(46)
We denote by T(n the subtree of an m rooted Cayley tree T containing the vertices from level -(m - 1) (the root -(m - 1)) to level n.
In most studies, M roots have most frequently been described as possessing two canals.
In this paper, we mainly consider an m rooted Cayley tree T ¯ C, N (see Figure 1).
Lemma 1 Let T be an m rooted Cayley tree, G = {0, 1,..., b - 1} be the finite state space.
In this paper, our main purpose is to extend Yang's [14] result to an m rooted Cayley tree.
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